Liquefaction: when an earthquake's violent shaking suddenly turns loose soft soil into the mud Aftershock: an earthquake that occurs after a larger earthquake in the same area Tsunamis: if the earthquake is strong enough, the water displaced by the quake forms large waves Base-isolated buildings: a building designed to reduce the amount of energy that reaches the building during an earthquake
Outline
How Earthquakes Cause Damage
Local Soil Conditions
when seismic waves move from hard, dense rock to loosely packed soil, they transmit their energy to the soil
loose soil shakes much more violently than the surrounding rock
the thicker the soil is, the more violently the shaking will be
this means that if your house is built on solid rock, the shaking will be less than the houses that are built on sandy soil
Liquefaction
1964, a powerful earthquake hit Anchorage, Alaska and cracked opened the ground
some of the cracks were 9 meters wide
some of the cracks were formed by liquefaction
liquefaction is likely to happen where the soil has too much moisture
as the ground gives way, buildings sink and pull apart
during the 1964 earthquake in Alaska, liquefaction
caused a landslide that swept thee entire housing development
Making Buildings Safer
Choice of Location
location of the building affects the type of damage it may suffer during an earthquake
that housing development went down the cliff and into the sea
steep slopes appose to the danger of landslides
a filled piece of land can shake violently
people should always check what their surroundings is like
the farther the structure is, the less shaking there will be
Construction methods
during an earthquake, a brick building or wood-frame building may collapse if it is not fixed
sometimes plywood sheets support frames of wooden buildings
to avoid damage caused by liquefaction is to build new homes on solid rock
bridges and highways dig down the soft soil and through the firmer ground
like the suspension of a car, the pads smooth the car from bumpy rides
during an earthquake, a base isolated building sways back and forth without any violent shaking
earthquakes indirectly cause floods and fire when the pipes break
automatic shut-off valves can be installed to cut off gas and water flow
Aftershocks
sometimes after an earthquake, there is an aftershock
buildings that are weakened by an earthquake, collapse during an aftershock
depends when an aftershock might happen
aftershocks may strike in hours,days or even months
Tsunamis
when an earthquake jolts the ocean floor, it starts to rise a little
it takes the water out of its way
if the earthquake is strong enough, the quake will start to form large waves
tsunamis spread out from an earthquake's epicenter and speeds across the ocean
the distance between the waves are 100 and 200 kilometers
some of the heights of the waves is about the height of a six-story building
Protecting Yourself During an Earthquake
the main dager of protecting ourself is falling objects
it means you need to crouch beneath a table and hold on to it so it won't fall
the table helps you protect from falling objects
if there is no table near you, then go crouch down to an inner wall
cover your neck with your hands
if you are outside, go to the middle of the street and stay out of the trees plus the electricity wires
Table of Contents
2.3 Earthquake Hazards and Safety
Vocabulary
Liquefaction: when an earthquake's violent shaking suddenly turns loose soft soil into the mud
Aftershock: an earthquake that occurs after a larger earthquake in the same area
Tsunamis: if the earthquake is strong enough, the water displaced by the quake forms large waves
Base-isolated buildings: a building designed to reduce the amount of energy that reaches the building during an earthquake
Outline
How Earthquakes Cause Damage
Making Buildings Safer
Protecting Yourself During an Earthquake
Diagram